The foundation date of the city of Utrecht is usually
equated to the erection of a Roman castellum called Traiectum (Latin for ford
or crossing) as part of the Limes Germanicus around the year 50. This square
fortress was located on a sideway of the main Roman Road from Lugdunum Batavorum
(Katwijk) to Colonia Ulpia Traiana (Xanten) and can still be located around the
Dom Square right in the heart of the city of Utrecht. It is located between the
Oude Gracht (Old Canal) and Kromme Nieuwe Gracht (Crooked New Canal). The
fortress was erected to defend the border of Germania Inferior against invading
Frisian and German Tribes from the north. A string of such forts ran along the
Rhine river from the coast to the foothills.
In red the castellum Traiectum on the map of the
historic city of Utrecht. In Yellow the old routes, these are not the Roman
road this ran further south from west to east.
The fortress was destroyed several times by invaders
and also the location on a low sand dune by the Rhine meant that floods were a
constant assault on its stability. The first fortress was constructed with
earth banks later topped with a palisade. Later fortresses were constructed
from wood with an embankment around it. The last of the castellae was built in
stone and bricks. The fortress also boasted a little harbour: the river itself
being the most reliable means of transport in the marshy terrain.
Looking at the current location within Utrecht the
castellum doesn't seem to be located on a major river. This position might seem
puzzling but one needs to take into account that the landscape looked very
different in Roman times. If we superimpose the old flow channels of the Rhine (Rhenus
in Latin) the image changes completely. Now the castellum of Traiectum is
located in a sharp bend of the river just before it forks and gives way to the
Vecht (Fectius in Latin). The fort itself is located on a low land dune and
probably had a moat on the land side thus being secure on all sides. In Roman
times this branch of the Rhine river with little slope was already silting up
as a result of the rise in sea level. Also a dam to lead more water into the
Waal river near Nijmegen (Noviomagus) decreased the flow in the Rhine. This in
turn lead to a dramatic rise in groundwater levels and the already marshy area
become difficult to navigate and go across as the rivers were turning into
narrow streams unfit for large vessels. Traiectum was finally abandoned around
270 AD. It seems though that people remained to live here.
The location makes more sense with the old river Rhine
projected on the map (in deep blue), showing the fort Traiectum (T) on a low
sand dune surrounded by water. These dunes (in amber) forced the water to take
several twists and turns and also provided a higher living space for local people
in a vicus (v) on either side of the fort. In light blue an even older branch
of the Rhine that had mostly silted up by Roman times. This shows how changeable
this landscape was.
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